Reservoir Water Column & Thermal Stratification
Ecosystem State:
Stable
Dissolved Oxygen (DO mg/L) vs Threshold
8.2 mg/L
Fish Population Biomass (%) & Mortality
100%
Limnological Dynamic Mechanics
Water volume is currently sufficient to buffer thermal loading. As drought severely curtails inflow and agricultural drawdown depletes total volume, thermal stratification collapses into a shallow, hypersaline, highly turbid soup where biochemical oxygen demand (BOD) rapidly strips dissolved oxygen below the lethal hypoxic threshold (DO < 2.0 mg/L), precipitating mass aquatic die-offs.